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THE EXCITATION OF LONG PERIOD SEISMIC-WAVES BY A SOURCE SPANNING A STRUCTURAL DISCONTINUITY

Abstract:
Simple theoretical results are obtained for the excitation of seismic waves by an indigenous seismic source in the case that the source volume is intersected by a structural discontinuity. In the long wavelength approximation the seismic radiation is identical to that of a point source placed on one side of the discontinuity or of a different point source placed on the other side of the discontinuity. The moment tensors of these two equivalent sources are related by a specific linear transformation and may differ appreciably both in magnitude and geometry. Either of these sources could be obtained by linear inversion of seismic data but the physical interpretation is more complicated than in the usual case. A source which involved no volume change would, for example, yield an isotropic component if, during inversion, it were assumed to lie on the wrong side of the discontinuity. The problem of determining the true moment tensor of the source is indeterminate unless further assumptions are made about the stress glut distribution; one way to resolve this indeterminancy is to assume proportionality between the integrated stress glut on each side of the discontinuity. -Author
Publication status:
Published

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Publisher copy:
10.1029/GL008i011p01129

Authors

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


Journal:
GEOPHYSICAL RESEARCH LETTERS More from this journal
Volume:
8
Issue:
11
Pages:
1129-1131
Publication date:
1981-01-01
DOI:
ISSN:
0094-8276


Language:
English
Pubs id:
pubs:187592
UUID:
uuid:188022b4-baa8-4f0d-8967-cd1d32cbe258
Local pid:
pubs:187592
Source identifiers:
187592
Deposit date:
2012-12-19
ARK identifier:

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